Report on Tangkuban Parahu (Indonesia) — 6 March-12 March 2013
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 6 March-12 March 2013
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2013. Report on Tangkuban Parahu (Indonesia). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 6 March-12 March 2013. Smithsonian Institution and US Geological Survey.
6.77°S, 107.6°E; summit elev. 2084 m
All times are local (unless otherwise noted)
According to news articles, an eruption from Tangkubanparahu on 4 March produced an ash plume that rose 500 m above the crater. An eight-minute-long eruption at 0559 on 7 March ejected ash 30 m above Ratu Crater.
Geologic Background. Gunung Tangkuban Parahu is a broad shield-like stratovolcano overlooking Indonesia's former capital city of Bandung. The volcano was constructed within the 6 x 8 km Pleistocene Sunda caldera, which formed about 190,000 years ago. The volcano's low profile is the subject of legends referring to the mountain of the "upturned boat." The Sunda caldera rim forms a prominent ridge on the western side; elsewhere the rim is largely buried by deposits of the current volcano. The dominantly small phreatic eruptions recorded since the 19th century have originated from several nested craters within an elliptical 1 x 1.5 km summit depression.
Source: The Jakarta Post